Petroleum Geology: North-West Europe and Global Perspectives—Proceedings of the 6th Petroleum Geology Conference
Petroleum Geology: North-West Europe and Global Perspectives–Proceedings of the 6th Petroleum Geology Conference represents key papers from the latest in a series of conferences that have become a focus for the most important issues in North-West European petroleum geology. As well as detailing the advances made in North-West Europe since the 5th Conference, this two-volume set also documents many generic and addresses the European experience in a global context.
The content focuses on the following items:
The global resource context
Exploration histories and future potential
Better recovery through better reservoir characterization
Atlantic margins: new insights, regional synthesis and large-scale tectonics
Deep-water plays and reservoirs
Understanding petroleum systems
Unlocking the future with innovative geophysics
The volumes are accompanied by an extensive selection of core photographs and seismic animations illustrating the many exploration models described. These books provide a significant reference to all geoscientists engaged in exploration and production in North-West Europe, to academic engaged in studying the area and to petroleum geologists interested in generic exploration models.
Evidence for a major sediment input point into the Faroe–Shetland Basin from the Kangerlussuaq region of southern East Greenland
Published:January 01, 2005
M. Larsen, A. G. Whitham, 2005. "Evidence for a major sediment input point into the Faroe–Shetland Basin from the Kangerlussuaq region of southern East Greenland", Petroleum Geology: North-West Europe and Global Perspectives—Proceedings of the 6th Petroleum Geology Conference, A. G. Doré, B. A. Vining
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Studies of the sedimentary succession in Kangerlussuaq, southern East Greenland suggest that a prominent sediment input point existed in the region in the Late Cretaceous-Palaeogene, which was controlled by a major northwest-southeast-oriented fault lineament. The presence of this sediment transfer path is supported by a number of observations. Firstly, the Cretaceous succession thickens towards the fault. This apparent thickening is due to post-depositional erosion of the succession and indicates a Late Maastrichtian-Palaeogene downthrow to the southwest. Secondly, Palaeogene sediments, which underlie the thick plateau basalt succession, are thickest along the axis of the sub-basin lying west of the fault...